BIOC58H3 Chapter 4: ch4.docx
Document Summary
We are currently in the quarternary ice agebegan 2 mya. Doesn"t feel like it cause were in the warm part-interglacial. Oligoscene- btw 35 and 15 mya earths temp was 4 degrees warmer because more co2. Major force of global climate came about by collision of indian and asian plates (55 mya). Caused an uplift to what became the tibetan plateu. Increased erosion, more silicate, more calcium silicate reacting with co2 precipating in form of calcium carbonate. First indications of shift in stability happened 42 mya in eocene. The end miocene- c4 plant better advantage of lower co2. Although lowering of co2 over tertiary facilitated speciation and rise of c4, lowering co2 itself cant explain their global spread at end of miocene: maybe tectonic activity, seasonal precipation, Studied teeth opposed to soils because feeding enhances isotope signal, soil more complex (combines both c13 and c12 )